Miranda or Uranus V is the fourteenth moon of Uranus in orbital order. It is also the fifth satellite to be discovered. It has a complex topography consisting of large canyons, cliffs, and rift valleys.[2][6]

Contents

Discovery

Gerard P. Kuiper discovered Miranda in 1948. He rejected at once naming the satellite after a son of Uranus, because earlier astronomers had already used Uranus' sons as names for Saturn's moons. He therefore followed the lead of Lassel and Herschel[1] and named Miranda after a character in one of the plays of William Shakespeare.[3]

When Voyager 2 flew by Uranus in 1986, Miranda was the closest moon to Voyager's flight path, and was therefore the one that Voyager 2 studied most closely. The Voyager team originally had not planned a mission to so small a moon, but could do nothing else; Voyager needed to make a precise hyperbolic pass at Uranus in order to steer toward Neptune, and Miranda happened to lie along the way. Yet in the end the Voyager scientists were grateful for the opportunity to study this remarkable object.[7][8]

Orbital characteristics

Miranda's orbit is one of the least eccentric of those of the five "major moons" of Uranus. While some of Uranus' moons have orbits that are less eccentric by an order of magnitude, Umbriel's orbit is significantly more eccentric than that of Miranda, and many of the other satellites have orbits more eccentric still.

More significantly, Miranda's orbit is inclined with respect to Uranus' equator by more than four degrees. This is the highest inclination among the orbits of the "major moons," although some of Uranus' moons have orbits that are inclined by more than forty-five degrees.

Rotational characteristics

Miranda orbits Uranus once every 33 hours, and is tidally locked to Uranus. This tidal locking does not allow Miranda to have a significant axial tilt.

Physical characteristics

Miranda's mass is less than 0.09% of the mass of Earth's Moon. At only 1200 kilograms per cubic meter, it is also one of the least dense, less dense even than the sun. Its density is closest to that of water, and so Miranda is believed to be composed mainly of ice with some rock.

Miranda has the most striking landscape of any spheroidal celestial body other than the earth. Its largest surface features are extremely striking in their bizarre variety and stark relief, almost as if Miranda were an object that someone pieced together out of scrap metal.[9] Twenty-kilometer canyons[7][8] give way to cratered regions[9] and other regions nearly devoid of craters. The mixture of geologically "old" and "young" regions is quite puzzling.[7]

Difficulties for uniformitarian theories

Shortly after the Visiting mission::Voyager 2 flyby, astronomers proposed that Miranda was shattered five times by collisions and then reassembled by mutual gravitational attraction.[10][8][9][7] But such a small moon would not be likely to survive even one collision, much less five. This theory is now out of favor.

The current favored theory is that Miranda was once in a 1:3 orbital resonance with Umbriel, and then escaped that resonance. While Miranda was resonating with Umbriel, its orbit gained in eccentricity and thus subjected it to tidal heating. To support that theory, astronomers point out that Miranda's orbit, inclined 4.22° from Uranus' equator, is more severely inclined than that of any other satellite in the Uranian system.[11][12][13] Some believe that this tidal heating caused an upwelling of subsurface ice that produced some of the most pronounced surface features.[14]

But this begs the question of how orbital resonances form, or how a satellite, once in such a resonance, would escape it. More to the point, however, is that the orbit of Miranda is not the most strikingly eccentric orbit in the Uranian system. Even among the major moons, that distinction belongs to Umbriel, not Miranda.

↑Tittemore, William C., and Wisdom, Jack. "Tidal evolution of the Uranian satellites II. An explanation of the anomalously high orbital inclination of Miranda." Icarus 78(1):63-89, March 1989. Accessed April 28, 2008. <doi:10.1016/0019-1035(89)90070-5>